Week 6 · Published May 31, 2026 · Paper 32 of 383
The Mid-Atlantic Ridge forms one of Earth's longest continuous uplift structures, displaying exceptional persistence across the Atlantic basin.
The ridge is interpreted through mantle upwelling, crustal generation, divergent plate boundaries, and seafloor spreading processes.
The ridge's continuity, geometry, and position can be cataloged as primary observations independent of explanatory models.
Observation-first analysis may reveal comparative relationships between ridge systems and other large-scale geological structures.